新疆石油地质 ›› 2008, Vol. 29 ›› Issue (2): 159-162.

• 油气勘探 • 上一篇    下一篇

鄂尔多斯盆地东南缘煤中沥青微量元素和稀土元素特征

李洪英1,2, 赫英2, 杨磊2, 刘养杰2   

  1. 1.中国地质科学院矿产资源研究所, 北京100037;
    2.西北大学地质学系, 西安710069
  • 收稿日期:2007-10-29 发布日期:2020-08-17
  • 作者简介:李洪英(1979-), 女, 陕西汉中人, 在读博士研究生, 地球化学,(Tel)010-88360672(E-mail)lihongyingy@163.com.
  • 基金资助:
    国家973重点基础研究发展计划项目, 多种能源矿产共存成藏(矿)机理与富集分布规律(2003CB214605)资助

Characteristics of Bitumen Trace Elements and Rare Earth Elements of Coal in Southeastern Margin of Ordos Basin

LI Hong-ying1,2, HE Ying2, YANG Lei2, LIU Yang-jie2   

  1. 1. Institute of Mineral Resources, Chinese Academy of Geosciences, Beijing 100037, China;
    2. Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China
  • Received:2007-10-29 Published:2020-08-17

摘要: 通过对鄂尔多斯盆地东南缘煤和煤层夹矸进行抽提, 得到其抽提物氯仿沥青A, 然后对氯仿沥青A 进行微量元素和稀土元素测试分析, 提供一些地球化学信息, 以此来揭示鄂尔多斯盆地东南缘煤中的一些地球化学特征。认为鄂尔多斯盆地东南缘煤的形成原始物可能主要来自上地壳。

关键词: 鄂尔多斯盆地, 煤, 沥青, 微量元素, 稀土元素

Abstract: Chloroform bitumen A has been extracted from coal and coal gangue in southeastern margin of Ordos basin. The trace elements and rare earth elements in it are tested and analyzed, which provide some geochemical information for revealing the geochemical characteristics of coal in this area. The study suggests that the original materials for forming coal in southeastern margin of Ordos basin are most likely from the upper crust.

Key words: Ordos basin, coal, bitumen, trace element, rare earth element

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